gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2010-1-2-0011gtcrust-102Research ArticleСОВРЕМЕННАЯ ГЕОДИНАМИКАRECENT GEODYNAMICSИЗМЕНЕНИЯ СТОЯНИЯ УРОВНЯ МОРЯ С I ВЕКА ПО XIII ВЕК И ИХ КЛИМАТИЧЕСКОЕ ЗНАЧЕНИЕSEA LEVEL CHANGES FROM THE I TO THE XIII CENTURIES AND THEIR CLIMATOLOGICAL SIGNIFICANCEМартЙоссиMartYossi

профессор,

31905, Хайфа

Professor,

31905, Haifa

yossimart@gmail.comИнститут морских исследований, Университет г. ХайфаИзраильRecanati Institute of Maritime Studies, University of HaifaIsrael20101309201512142147Copyright © Март Й., 20152015Март Й.Mart Y.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://www.gt-crust.ru/jour/article/view/102

Корреляции между археологическими материалами и геологическими наблюдениями показывают, что регион портового города Кейсария в центральной части Израиля в течение последних 2000 лет был относительно стабилен. Такая стабильность и малый диапазон суточных приливно-отливных колебаний уровня моря позволяют провести реконструкцию разных уровней моря в рамках ряда археологических временных периодов с учетом климатической значимости. По нашему мнению, в течение 2000-летнего периода стояние уровня моря, а также климат были аналогичны современным. Уровень моря был выше в VII–VIII веках н.э., а климат, возможно, был теплее; в ХII–ХIII веках н.э. уровень моря был ниже, а климат холоднее. Высказывается мнение, что пред- положение о том, что современное глобальное потепление вызвано антропогенным воздействием, нуждается в убедительных доказательствах. Вместе с тем, весьма вероятной представляется связь между современными значительными разрушениями коралловых рифов и антропогенными факторами, вызывающими повышение содержания углекислого газа в атмосфере.

Correlation between archaeological ruins and geological observations show that the region of the port city of Caesarea in central Israel has been stable during the last 2000 years. This stability, and the low range of the diurnal tidal variations of sea level, attributes global climatic significance to the reconstructions of various sea levels during several clear archaeological time-frames. It seems that while 2000 years ago sea level, and therefore also climate, was similar to the present one. Sea level was higher in the VII–VIII Centuries AD, and the climate was probably warmer, and sea level was lower, and the climate colder, in the ХII–ХIII Centuries AD. Consequently it is suggested that the presumption that the present global climatic warming in anthropogenic requires strong supporting evidence. On the other hand, the link between recent heavy damages to coral reefs and the anthropogenic activities that caused the rise in atmospheric CO2 content seems quite likely.

изменение уровня моряактивная тектоникаизменение климатаsea level changeactive tectonicsclimate changeReferencesCane M.A, Molnar P. Closing of the Indonesian seaway as a precursor to east African aridification around 3–4 million years ago // Nature. – 2001. – V. 411. – P. 157–162.Cane M.A, Molnar P. Closing of the Indonesian seaway as a precursor to east African aridification around 3–4 million years ago // Nature. – 2001. – V. 411. – P. 157–162.Driscoll N.W., Haug G.H. A Short Circuit in Thermohaline Circulation: A Cause for Northern Hemisphere Glaciation? // Science. – 1998. – V. 282, № 5388. – P. 436–438.Driscoll N.W., Haug G.H. A Short Circuit in Thermohaline Circulation: A Cause for Northern Hemisphere Glaciation? // Science. – 1998. – V. 282, № 5388. – P. 436–438.Emiliani C. Temperature and age analysis of deepsea cores // Science. – 1957. – V. 125. – P. 383–385.Emiliani C. Temperature and age analysis of deepsea cores // Science. – 1957. – V. 125. – P. 383–385.Fagan B. The Little Ice Age. – New York: Basic Books Inc., 2000. – 146 p.Fagan B. The Little Ice Age. – New York: Basic Books Inc., 2000. – 146 p.Fine M., Tchernov D. Scleractinian Coral Species Survive and Recover from Decalcification // Science. – 2007. – V. 315. – P. 1811.Fine M., Tchernov D. Scleractinian Coral Species Survive and Recover from Decalcification // Science. – 2007. – V. 315. – P. 1811.Haug G.H., Tiedemann R., Zahn R., Ravelo A.C. Role of Panama uplift on oceanic freshwater balance // Geology. – 2001. – V. 29. – P. 207–210.Haug G.H., Tiedemann R., Zahn R., Ravelo A.C. Role of Panama uplift on oceanic freshwater balance // Geology. – 2001. – V. 29. – P. 207–210.Imbrie J., Imbrie K.P. Ice Ages: Solving the Mystery. – Short Hills NJ: Enslow Publishers, 1979. – 231 p.Imbrie J., Imbrie K.P. Ice Ages: Solving the Mystery. – Short Hills NJ: Enslow Publishers, 1979. – 231 p.Issar A.S. Climate Changes during the Holocene and their Impact on Hydrological Systems. – Cambridge: Cambridge University Press, 2003. – 187 p.Issar A.S. Climate Changes during the Holocene and their Impact on Hydrological Systems. – Cambridge: Cambridge University Press, 2003. – 187 p.Mart Y., Perecman I. Neotectonic activity along the coast in Caesarea, central Israel // Tectonophysics. – 1996. – V. 254. – P. 139–153.Mart Y., Perecman I. Neotectonic activity along the coast in Caesarea, central Israel // Tectonophysics. – 1996. – V. 254. – P. 139–153.Milankovitch M. Théorie Mathématique des Phénomènes Thermiques produits par la Radiation Solaire. – Paris: Gauthier-Villars, 1920.Milankovitch M. Théorie Mathématique des Phénomènes Thermiques produits par la Radiation Solaire. – Paris: Gauthier-Villars, 1920.Neev D. Tectonic evolution of the Middle East and the Levantine basin (Southeastern Mediterranean) // Geology. – 1975. – V. 3. – P. 683–686.Neev D. Tectonic evolution of the Middle East and the Levantine basin (Southeastern Mediterranean) // Geology. – 1975. – V. 3. – P. 683–686.Neev D., Almagor G., Arad A., Ginzburg A., Hall J.K. The geology of the Southeastern Mediterranean // Geological Survey of Israel Bulletin. – 1976. – V. 68. – P. 1–51.Neev D., Almagor G., Arad A., Ginzburg A., Hall J.K. The geology of the Southeastern Mediterranean // Geological Survey of Israel Bulletin. – 1976. – V. 68. – P. 1–51.Neev D., Bakler N., Emery K.O. Mediterranean Coasts of Israel and Sinai. – New York: Taylor and Francis, 1987. – 130 p.Neev D., Bakler N., Emery K.O. Mediterranean Coasts of Israel and Sinai. – New York: Taylor and Francis, 1987. – 130 p.Nir Y., Eldar I. Ancient wells and their geoarchaeological significance in detecting tectonics of the Israel Mediterranean coastline region // Geology. – 1987. – V. 15. – P. 3–6.Nir Y., Eldar I. Ancient wells and their geoarchaeological significance in detecting tectonics of the Israel Mediterranean coastline region // Geology. – 1987. – V. 15. – P. 3–6.Pirazzoli P.A. World Atlas of Sea-Level Changes. – New York: Elsevier, 1992.Pirazzoli P.A. World Atlas of Sea-Level Changes. – New York: Elsevier, 1992.Raban A. The Harbour of Sebastos (Caesarea Maritima) in its Roman Mediterranean Context / Edited by M. Artzy, B. Goodman, Z. Gal. – Brit. Arch. Rep. (BAR) – S1930, 2009.Raban A. The Harbour of Sebastos (Caesarea Maritima) in its Roman Mediterranean Context / Edited by M. Artzy, B. Goodman, Z. Gal. – Brit. Arch. Rep. (BAR) – S1930, 2009.Sella G.F., Stein S., Dixon T.H., Craymer M., James T.S., Mazzotti S., Dokka R.K. Observation of glacial isostatic adjustment in «stable» North America with GPS // Geophysical Research Letters. – 2007. – V. 34. – L02306. – doi:10.1029/2006GL027081.Sella G.F., Stein S., Dixon T.H., Craymer M., James T.S., Mazzotti S., Dokka R.K. Observation of glacial isostatic adjustment in «stable» North America with GPS // Geophysical Research Letters. – 2007. – V. 34. – L02306. – doi:10.1029/2006GL027081.Sivan D., Lambeck K., Toueg R., Raban A., Porat Y., Shirman B. Ancient coastal wells of Caesarea Maritima, Israel, an indicator for sea level changes during the last 2000 years // Earth and Planetary Science Letters. – 2004. – V. 222. – P. 315–330.Sivan D., Lambeck K., Toueg R., Raban A., Porat Y., Shirman B. Ancient coastal wells of Caesarea Maritima, Israel, an indicator for sea level changes during the last 2000 years // Earth and Planetary Science Letters. – 2004. – V. 222. – P. 315–330.Stanley D.J. Subsidence in the northeastern Nile delta: rapid rates, possible causes, and consequences // Science. – 1988. – V. 240. – P. 497–500.Stanley D.J. Subsidence in the northeastern Nile delta: rapid rates, possible causes, and consequences // Science. – 1988. – V. 240. – P. 497–500.

The authors declare that there are no conflicts of interest present.